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转身丶忘不掉

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[求助] 英语水平有限,求帮忙翻译一下,谢谢 附图

2. Experimental
2.1. Material and experimental conditions
   The experiments, which were modified in order to be able to control redox condition, were carried out by an in-diffusion method (Sato, 1998). Table 1 shows the experimental conditions for the diffusion experiments.
   A Na bentonite, Kunigel-V1R (Kunimine Industries), of which much data regarding fundamental properties have been reported up to the present, was used in a series of diffusion experiments. The major constituent clay minerals of the bentonite are Nasmectite and chalcedony, which makes up 46–49 and 37–38 wt.%, respectively (Ito et al., 1993,1994). Some other minor minerals, such as quartz, plagioclase, calcite, dolomite, analcite and pyrite are also contained as impurities. The quantitative details of the minerals are described in the literature (Ito et al.,1993, 1994).

英语水平有限,求帮忙翻译一下,谢谢 附图
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RXMCDM: 金币+1, 多谢应助! 2014-09-11 13:11:04
转身丶忘不掉: 金币+8, ★★★★★最佳答案 2014-09-12 07:38:17
2,实验
2.1. 材料和实验条件
为了能够控制氧化还原的条件,实验进行了改进并用内扩散法进行(Sato, 1998)。表1列出了扩散实验的实验条件为。
用钠膨润土和Kunigel-V1R(Kunimine工业公司,其中有关Kunigel-V1R基本属性的数据量已经报道)进行了一系列扩散实验。膨润土的主要成分粘土矿物是Nasmectite和玉髓,分别占46-49%和37-38%(重量%)(Ito et al., 1993,1994)。其他一些次要的矿物,例如石英,长石,方解石,白云,方沸石和黄铁矿等被视为杂质。矿物质的详细定量资料在文献中有描述 (Ito et al.,1993, 1994)。
2楼2014-09-11 12:50:14
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